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  • 1
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 92.0308 ; AWI G1-96-0008
    Type of Medium: Monograph available for loan
    Pages: XIX, 955 S. : 393 Fig.
    ISBN: 3540527842
    Classification:
    Petrology, Petrography
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 92.0283
    Type of Medium: Monograph available for loan
    Pages: X, 628 S.
    ISBN: 3540547436
    Classification:
    Petrology, Petrography
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Publication Date: 1991-10-01
    Print ISSN: 1435-9529
    Electronic ISSN: 1435-9537
    Topics: Geosciences
    Published by Springer
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  • 4
    Publication Date: 1983-07-01
    Print ISSN: 0012-0189
    Topics: Geosciences
    Published by Schweizerbart
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  • 5
    Publication Date: 1990-03-01
    Print ISSN: 0025-3227
    Electronic ISSN: 1872-6151
    Topics: Geosciences
    Published by Elsevier
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  • 6
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    Springer
    In:  Senckenbergiana Lethaea, 48 (3/4). pp. 359-379.
    Publication Date: 2017-01-24
    Description: Am Süd-Ausgang des Roten Meeres entstehen unter idealen Wachstumsbedingungen fast reine Korallen-Saumriffe, die als dünne Platten oft kilometerweit mit einer Geschwindigkeit von Zentimetern pro Jahr auf ihrem Schutt von der Küste horizontal gegen das Meer vorwachsen. Aufgetauchte Saumrifte, ein flacher Bootskanal oder abradierte Riffoberflächen weisen auf pleistozäne und jüngere Meeresspiegelschwankungen bzw. tektonische Verstellungen hin. Von einer gewissen Breite an bilden sich auf den Riffen Inseln in Form langgestreckter Rücken aus Korallensand, hinter denen sich stellenweise Mangrove ansiedelt oder Salze in flachen Lagunen abscheiden. Schließlich kann der Strand auf das Saumriff vorverlegt und dieses in die Küstenebene einbezogen werden.
    Type: Article , PeerReviewed
    Format: text
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  • 7
    Publication Date: 2022-07-08
    Description: The study of textural, structural, chemical, and physical properties of fine-grained recent marine sediments leads to the conclusion that only a few compositional factors are responsible for significant changes in mass physical characteristics in the upper meters below sea bottom. Fossil-induced porosity (text fig. 6) increases water content and liquid limit. It also seems to have partially influenced the plastic limit and plasticity index of calcareous sandy silts from the Red Sea and the western Gulf of Aden so that they become similar to the montmorillonite rich prodelta clays from the Nile Delta. Diagrams based on liquid limit and plasticity loose their original meaning in these cases (text fig. 7 a). Activity of sediments rich in microorganisms can be higher than that of montmorillonitic clay (text fig. 7b). The shear strength-depth relationship of normally consolidated sediments (text fig. 8 a) is surprisingly little influenced by changes in sand or clay content and clay mineralogy. Only high lime content, submarine erosion and beginning cementation increase the strength considerably (part of curves in text fig. 8 b ). Erosional disconformities near the present surface can be deduced from the strength-depth curve when as little as 1 or 2 m sediment have been removed (text fig. 9). Flat or irregular strength-depth curves (text fig. 8 b, curves B and GO) indicate beginning cementation and probably discontinuous sedimentation, provided the composition of the material remains in some degree constant. In our samples diagenetic pyrite, but no recristallisation of carbonates could be detected under the microscope. Underconsolidation and excess pore-water pressure, factors which tend to foster submarine slides, mud lumps, and diapiric folding, seem to be restricted to areas with mainly rapidly deposited, homogeneous or layered sediments. But where an abundance of burrowing organisms increases the vertical permeability of the sediment, normal consolidation and stable deposits are to be expected, at least in the upper meters below the present surface. According to 14C-determinations on calcareous microorganisms the rate of deposition of the investigated sediments seems to range from 26 to 167 cm per 1000 years.
    Type: Article , PeerReviewed
    Format: text
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  • 8
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    PANGAEA
    In:  Supplement to: Curray, Joseph R; Moore, David G; Kelts, Kerry; Einsele, Gerhard (1982): Tectonics and Geological History of the Passive Continental Margin at the Tip of Baja California. In: Curray, J.R.; Moore, D.G.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXIV, 1089-1136, https://doi.org/10.2973/dsdp.proc.64.150.1982
    Publication Date: 2023-08-28
    Description: he three-site Leg 64 Deep Sea Drilling transect at the tip of the Peninsula of Baja California straddled the transition from continental to oceanic crust. The outer site, 474, penetrated mainly mud turbidites and bottomed in "middle" Pliocene oceanic crust about 3 m.y. old. Two sites on the lower continental slope penetrated hemipelagic muddy sediments, a thin section of low-oxygen, phosphoritic, and glauconitic sediments, and a metamorphic cobble conglomerate; one of the sites, 476, bottomed in deeply weathered granite. The oldest marine sediments at this site are early Pliocene, about 4.5 m.y. old. Depth indicators in these holes suggest that all sites were in almost 1000 meters of water by the time oceanic crust was first generated and sea-floor spreading began. Block faulting, subsidence, and deposition of marine sediments on continental crust had preceded the start of sea-floor spreading. Close examination of lineated magnetic anomalies demonstrates that the transition from continental to oceanic crust in this region is diachronous, as early as 4.9 m.y. in some places, but as young as 3.2 m.y. along the line of the transect. We propose a geological history scenario which involves termination of subduction along the western margin of Baja California at 12.5 Ma, a period of transform motion between the Pacific and North American plates along the Tosco Abreojos Transform Fault zone along the west side of Baja California, and a jump of the Pacific-North American plate edge to the alignment of the Gulf at 5.5 Ma. Between 5.5 Ma and about 3.2 Ma, separation of the blocks occurred locally by sea-floor spreading, but elsewhere by "diffuse extension", largely involving listric normal faulting and thinning of the continental crust, accompanied by subsidence and marine inundation. Thus, the plate edge system in the mouth and southern part of the Gulf evolved as early as 5.5 Ma, but the transition from rifting to drifting was diachronous, starting only 3.2 Ma along the line of the transect.
    Keywords: Argo; BAC-17; BAC-44; BAC-58; BAC-59; BAC-61; BACANYON; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GUAY-1D; GUAY-2D; GUAY-5D; GUAYAMAS; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Substrate type; Thomas Washington; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 9
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    Unknown
    PANGAEA
    In:  Supplement to: Einsele, Gerhard (1982): Mass physical properties of Pliocene to Quaternary sediment in the Gulf of California, Deep Sea Drilling Project Leg 64. In: Curray, JR; Moore, DG; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 64, 529-542, https://doi.org/10.2973/dsdp.proc.64.108.1982
    Publication Date: 2023-09-07
    Description: The Pliocene-Quaternary sediments that we drilled at eight sites in the Gulf of California consist of silty clays to clayey silts, diatomaceous oozes, and mixtures of both types. In this chapter I have summarized various measurements of their physical properties, relating this information to burial depth and effective overburden pressure. Rapid deposition and frequent intercalations of mud turbidites may cause underconsolidation in some cases; overconsolidation probably can be excluded. General lithification begins at depths between 200 and 300 meters sub-bottom, at porosities between 55 and 60% (for silty clays) and as high as 70% (for diatomaceous ooze). Diatom-rich sediments have low strength and very high porosities (70-90%) and can maintain this state to a depth of nearly 400 meters (where the overburden pressure = 1.4 MPa). The field compressibility curves of all sites are compared to data published earlier. Where sediments are affected by basaltic sills, these curves clearly show the effects of additional loading and thermal stress (diagenesis near the contacts). Strength measurements on well-preserved hydraulic piston cores yielded results similar to those obtained on selected samples from standard drilling. Volumetric shrinkage dropped to low values at 100 to 400 meters burial depth (0.3 to 2.0 MPa overburden pressure). Porosity after shrinkage depends on the composition of sediments.
    Keywords: 64-474A; 64-476; 64-477A; 64-479; 64-481A; Deep Sea Drilling Project; Density, wet bulk; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Hamilton frame velocimeter, Boyce (1976); Impedance, specific; Latitude of event; Leg64; Longitude of event; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/TERRACE; Quality of orientation; Rock type; Sample code/label; see reference(s); Sonic velocity
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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